SM54B-04
Chang’e-3 Extreme Ultraviolet Camera Observations of the Dynamics of the Earth’s Plasmasphere
Friday, 18 December 2015: 17:00
2018 (Moscone West)
Xiaoxin Zhang1, Fei He2, Bo Chen2, Mei-Ching Hannah Fok3, Hua-Ning Wang4, Chao Shen5 and Jinsong Ping6, (1)CMA China Meteorological Administration, Beijing, China, (2)CIOMP Changchun Institute of Optics, Fine Mechanics and Physics, CAS, Changchun, China, (3)NASA Goddard Space Flight Center, Greenbelt, MD, United States, (4)National Astronomical Observatories, Chinese Academy of Sciences, Beijing, China, (5)Chinese Academy of Sciences, Beijing, China, (6)National Astronomical Observatories, Beijing, China
Abstract:
The Moon-based Extreme Ultraviolet Camera (EUVC) aboard China’s Chang’e-3 (CE-3) lunar lander has successfully imaged the global plasmasphere on the Moon for the first time through detecting the resonantly scattered sunlight by plasmaspheric He+ at 30.4 nm with a spatial resolution of 0.1 RE and a time resolution of 10 min. The characteristics and the analyzing methods of the EUVC images are introduced in detail in this report. The plasmapause locations on the magnetic equator are reconstructed with the Minimum L Algorithm and are quantitatively compared with those extracted from in-situ observations by DMSP, THEMIS, and RBSP satellites. Then the plasmapause evolutions during substorms on February 21 2014 and April 21 2014 are investigated. It is found that the evolutions of plasmapause correlate well in both universal time and magnetic local time with the equatorial boundaries of auroral oval during substorms. During these two cases, the solar-wind-driven convection and the geomagnetic activity are relatively weak and steady, and the plasmapause motions can reliably be attributed to the substorms. It is proposed that correlations between the auroral signatures and the plasmapause motions may be due to the generation and Earthward-propagation of dipolarization front and resultant pitch angle scattering. In future work, we will search more in-situ and remote sensing data in both the plasmasphere and the magnetotail regions to investigate the correlations between the plasmaspheric erosions, the dipolarization fronts, and the energetic ions injections.